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Map showing flow field changes...
Map showing flow field changes
Map showing flow field changes
Map showing flow field changes

This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area of the flow on April 3 is shown in pink, while widening and advancement of the flow as of April 9 is shown in red. We were not able to map some parts of the flow field with breakouts today due to poor weather, and these areas are denoted in boxes.

This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area of the flow on April 3 is shown in pink, while widening and advancement of the flow as of April 9 is shown in red. We were not able to map some parts of the flow field with breakouts today due to poor weather, and these areas are denoted in boxes.

A closer look at the leading tip of the farthest downslope breakout...
leading tip of the farthest downslope breakout. The tip of the bre...
leading tip of the farthest downslope breakout. The tip of the bre...
leading tip of the farthest downslope breakout. The tip of the bre...

A closer look at the leading tip of the farthest downslope breakout. The tip of the breakout was burning forest, and was 6.9 km (4.3 miles) northeast of the June 27th vent on Pu‘u ‘Ō‘ō.

Scattered breakouts northeast of Pu‘u ‘Ō‘ō continue...
Scattered breakouts NE of Pu‘u ‘Ō‘ō continue
Scattered breakouts NE of Pu‘u ‘Ō‘ō continue
Scattered breakouts NE of Pu‘u ‘Ō‘ō continue

Breakouts continue northeast of Pu‘u ‘Ō‘ō in three main areas: 1) at the northern base of Pu‘u ‘Ō‘ō cone, 2) north of Pu‘u Kahauale‘a and 3) about 6 km (4 miles) northeast of Pu‘u ‘Ō‘ō. This photograph looks east and shows the breakout about 6 km from Pu‘u ‘Ō‘ō.

Breakouts continue northeast of Pu‘u ‘Ō‘ō in three main areas: 1) at the northern base of Pu‘u ‘Ō‘ō cone, 2) north of Pu‘u Kahauale‘a and 3) about 6 km (4 miles) northeast of Pu‘u ‘Ō‘ō. This photograph looks east and shows the breakout about 6 km from Pu‘u ‘Ō‘ō.

This photograph looks upslope and shows another narrow lobe on the ...
This photograph looks upslope and shows another narrow lobe on the ...
This photograph looks upslope and shows another narrow lobe on the ...
This photograph looks upslope and shows another narrow lobe on the ...

This photograph looks upslope and shows another narrow lobe on the breakout that is roughly 6 km (4 miles) northeast of Pu‘u ‘Ō‘ō. This lobe was moving along the south margin of the June 27th flow.

This photograph looks upslope and shows another narrow lobe on the breakout that is roughly 6 km (4 miles) northeast of Pu‘u ‘Ō‘ō. This lobe was moving along the south margin of the June 27th flow.

Map showing flow field changes...
Map showing flow field changes
Map showing flow field changes
Map showing flow field changes

This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area of the flow on March 24 is shown in pink, while widening and advancement of the flow as of April 3 is shown in red.

This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area of the flow on March 24 is shown in pink, while widening and advancement of the flow as of April 3 is shown in red.

Map show flow field with thermal overlays...
Map show flow field with thermal overlays
Map show flow field with thermal overlays
Map show flow field with thermal overlays

This map overlays georegistered mosaics of thermal images collected during a helicopter overflight of the three areas of breakouts near Pu‘u ‘Ō‘ō on April 3. The perimeter of the flow at the time the imagery was acquired is outlined in yellow.

This map overlays georegistered mosaics of thermal images collected during a helicopter overflight of the three areas of breakouts near Pu‘u ‘Ō‘ō on April 3. The perimeter of the flow at the time the imagery was acquired is outlined in yellow.

A closer look at the new pit in the western portion of Pu‘u ‘Ō‘ō Cr...
new pit in the western portion of Pu‘u ‘Ō‘ō
new pit in the western portion of Pu‘u ‘Ō‘ō
new pit in the western portion of Pu‘u ‘Ō‘ō

A closer look at the new pit in the western portion of Pu‘u ‘Ō‘ō Crater. Views inside the crater with the naked eye were obscured by thick fume, but the thermal images (right) revealed two areas of ponded lava, separated by a pile of collapse rubble, deep within the pit.

A closer look at the new pit in the western portion of Pu‘u ‘Ō‘ō Crater. Views inside the crater with the naked eye were obscured by thick fume, but the thermal images (right) revealed two areas of ponded lava, separated by a pile of collapse rubble, deep within the pit.

Pu‘u ‘Ō‘ō — Flow
Pu‘u ‘Ō‘ō — Flow
Pu‘u ‘Ō‘ō — Flow
Pu‘u ‘Ō‘ō — Flow

A closer look at the lava flow field near Pu‘u ‘Ō‘ō. Pu‘u ‘Ō‘ō is in the upper left portion of the photograph. Slightly above and to the right of the center of the photograph, the light colored area of lava is the active breakout (which started on February 21) on the north flank of Pu‘u ‘Ō‘ō.

A closer look at the lava flow field near Pu‘u ‘Ō‘ō. Pu‘u ‘Ō‘ō is in the upper left portion of the photograph. Slightly above and to the right of the center of the photograph, the light colored area of lava is the active breakout (which started on February 21) on the north flank of Pu‘u ‘Ō‘ō.

In the time since our last overflight (March 24), a new collapse pi...
New collapse pit has formed in the western portion of Pu‘u ‘Ō‘ō
New collapse pit has formed in the western portion of Pu‘u ‘Ō‘ō
New collapse pit has formed in the western portion of Pu‘u ‘Ō‘ō

In the time since our last overflight (March 24), a new collapse pit has formed in the western portion of Pu‘u ‘Ō‘ō Crater. This circular pit can be seen in the lower left portion of the photograph, and measures about 27 m (roughly 90 ft) in diameter. Numerous hot cracks were observed in this general area during previous visits on foot.

In the time since our last overflight (March 24), a new collapse pit has formed in the western portion of Pu‘u ‘Ō‘ō Crater. This circular pit can be seen in the lower left portion of the photograph, and measures about 27 m (roughly 90 ft) in diameter. Numerous hot cracks were observed in this general area during previous visits on foot.

Breakouts persist northeast of Pu‘u ‘Ō‘ō...
Breakouts persist NE of Pu‘u ‘Ō‘ō
Breakouts persist NE of Pu‘u ‘Ō‘ō
Breakouts persist NE of Pu‘u ‘Ō‘ō

Breakouts remain active in three general areas near Pu‘u ‘Ō‘ō: 1) at the northern base of Pu‘u ‘Ō‘ō, 2) just north of Kahauale‘a, and 3) the most distal breakout, about 6 km (4 miles) northeast of Pu‘u ‘Ō‘ō. This photograph shows much of the most distal breakout, a portion of which was burning forest. Pu‘u ‘Ō‘ō can be seen near the top of the photograph.

Breakouts remain active in three general areas near Pu‘u ‘Ō‘ō: 1) at the northern base of Pu‘u ‘Ō‘ō, 2) just north of Kahauale‘a, and 3) the most distal breakout, about 6 km (4 miles) northeast of Pu‘u ‘Ō‘ō. This photograph shows much of the most distal breakout, a portion of which was burning forest. Pu‘u ‘Ō‘ō can be seen near the top of the photograph.

The breakout north of Kahauale‘a has one lobe that has traveled alo...
The breakout north of Kahauale‘a has one lobe that has traveled alo...
The breakout north of Kahauale‘a has one lobe that has traveled alo...
The breakout north of Kahauale‘a has one lobe that has traveled alo...

The breakout north of Kahauale‘a has one lobe that has traveled along the west side of the perched lava channel that was active in late 2007. This breakout consists of blue glassy pāhoehoe, which is easily visible in the photograph on the left. The white box shows the rough extent of the thermal image on the right.

The breakout north of Kahauale‘a has one lobe that has traveled along the west side of the perched lava channel that was active in late 2007. This breakout consists of blue glassy pāhoehoe, which is easily visible in the photograph on the left. The white box shows the rough extent of the thermal image on the right.

Comparing Kalapana and June 27th flows provides perspective on lava...
Comparing Kalapana and June 27th flows
Comparing Kalapana and June 27th flows
Comparing Kalapana and June 27th flows

The pāhoehoe flows that moved through Kalapana in 1990 (left) were hotter, more fluid, and faster-moving than the lava flow that reached to within 155 m (170 yds) of Pāhoa Village Road in October 2014 (right). USGS photos.

The pāhoehoe flows that moved through Kalapana in 1990 (left) were hotter, more fluid, and faster-moving than the lava flow that reached to within 155 m (170 yds) of Pāhoa Village Road in October 2014 (right). USGS photos.

Map showing flow field changes...
Map showing flow field changes
Map showing flow field changes
Map showing flow field changes

This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area of the flow on March 10, before shutting down near Pāhoa, is shown in pink, while widening and advancement of the flow based on satellite imagery from April 1 is shown in red.

This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area of the flow on March 10, before shutting down near Pāhoa, is shown in pink, while widening and advancement of the flow based on satellite imagery from April 1 is shown in red.

There are several incandescent and outgassing hornitos on the floor...
There are several incandescent and outgassing hornitos on the floor...
There are several incandescent and outgassing hornitos on the floor...
There are several incandescent and outgassing hornitos on the floor...

There are several incandescent and outgassing hornitos on the floor of Pu‘u ‘Ō‘ō's crater, including the one shown here, which is at the northeast edge of the crater. Recent flows from the hornito appear black.

There are several incandescent and outgassing hornitos on the floor of Pu‘u ‘Ō‘ō's crater, including the one shown here, which is at the northeast edge of the crater. Recent flows from the hornito appear black.

Map showing flow field changes...
Map showing flow field changes
Map showing flow field changes
Map showing flow field changes

This map shows the changes to Kīlauea's active East Rift Zone lava flow field. The area of the flow on March 17 is shown in pink, while widening and advancement of the flow as of March 24 is shown in red. Small changes west of Pu‘u Kahauale‘a are not shown, as that part of the flow field was hidden by Pu‘u ‘Ō‘ō's gas plume at the time of mapping.

This map shows the changes to Kīlauea's active East Rift Zone lava flow field. The area of the flow on March 17 is shown in pink, while widening and advancement of the flow as of March 24 is shown in red. Small changes west of Pu‘u Kahauale‘a are not shown, as that part of the flow field was hidden by Pu‘u ‘Ō‘ō's gas plume at the time of mapping.

Active breakouts near Pu‘u ‘Ō‘ō
Active breakouts near Pu‘u ‘Ō‘ō
Active breakouts near Pu‘u ‘Ō‘ō
Active breakouts near Pu‘u ‘Ō‘ō

Breakouts are active in three general areas near Pu‘u ‘Ō‘ō: at the northern base of Pu‘u ‘Ō‘ō, north Kahauale‘a, and about 6 km (4 mi) northeast of Pu‘u ‘Ō‘ō. The distal breakout and the breakout north of Kahauale‘a are both burning forest. There is no eruptive activity downslope from the distal breakout (nothing active near Pāhoa).

Breakouts are active in three general areas near Pu‘u ‘Ō‘ō: at the northern base of Pu‘u ‘Ō‘ō, north Kahauale‘a, and about 6 km (4 mi) northeast of Pu‘u ‘Ō‘ō. The distal breakout and the breakout north of Kahauale‘a are both burning forest. There is no eruptive activity downslope from the distal breakout (nothing active near Pāhoa).

Mauna Loa: Quiet for many years, but not to be forgotten...
Mauna Loa: Quiet for many years, but not to be forgotten
Mauna Loa: Quiet for many years, but not to be forgotten
Mauna Loa: Quiet for many years, but not to be forgotten

‘A‘ā lava flows erupt from the Northeast Rift Zone of Mauna Loa on March 25, 1984—the first day of the volcano's most recent eruption. USGS photo.

Re-establishing VLF eruption rate monitor...
Re-establishing VLF eruption rate monitor
Re-establishing VLF eruption rate monitor
Re-establishing VLF eruption rate monitor

After establishing an appropriate location to resume VLF measurements over the June 27th lava tube to estimate the cross-sectional area of lava within the tube, HVO geologists make the measurements, sometimes requiring walking through volcanic gases.

After establishing an appropriate location to resume VLF measurements over the June 27th lava tube to estimate the cross-sectional area of lava within the tube, HVO geologists make the measurements, sometimes requiring walking through volcanic gases.

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